Forecast new snow amounts and freezing levels are uncertain, due to weather models variability. Watch how high freezing levels climb, and avoid slopes that become moist or wet.
Confidence
Moderate - Freezing levels are uncertain
Weather Forecast
Light snow (3-5 cm) overnight with light southerly winds and freezing levels at about 1600 metres in the south and closer to 1000 metres in the north. Another 5-8 cm during the day on Thursday with increasing southwest winds and freezing levels up to about 1800 metres in the south. On Friday, expect flurries, light winds, and periods of broken skies. Freezing levels should rise up to about 1600 metres during the day and then fall to valley bottoms by Saturday morning. Scattered cloud with light southerly winds on Saturday, freezing level rising again to at least 1500 metres.
Avalanche Summary
On Tuesday we had reports of explosives controlled slab avalanches up to size 3.0 in the west central part of the region, and thin new windslabs in the north that were skier controlled, as well as a size 2.5 deep persistent slab avalanche was reported that probably released on Monday on a west aspect in the alpine. On Monday we had reports of natural wind slab avalanches up to size 2.0, and one wind slab in the alpine that stepped down to a persistent week layer on an east aspect resulting in a size 3.0 avalanche.
Snowpack Summary
Approximately 10 cm of new snow arrived by Tuesday morning. Moderate to strong westerly winds transported the new snow into wind slabs in the alpine and at treeline. The new snow will overlie wind slabs which formed over the past few days. About 15-40 cm below the surface, you'll likely find a melt freeze crust which exists in most places except for in high elevation shaded terrain. In general there seems to be a reasonable bond between the crust and the overlying snow. I'd still keep an eye on this interface as it has become reactive on some features. The early January surface hoar/ facet layer is typically down 70-120 cm. Avalanche activity at this interface has tapered-off over the past week, but I'd be reluctant to trust this potentially destructive layer just yet. In general, the lower snowpack is well settled and strong, apart from some thin snowpack areas where basal facets exist.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.
Loose Wet
Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.